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The Central and Southern Mixed Grasslands ecoregion has a north-south orientation, spanning central Nebraska, central Kansas, western Oklahoma, and north-central Texas. It separates the Tall-Grass Prairie and the Central Forests/Grassland Transition Zone from the Western Short Grasslands. Essentially, this region is a broad ecotone that covers slightly more than 282,000 km2. It is distinguished from the Northern Mixed Grasslands by warmer temperatures and a much longer growing season, and from the adjacent tallgrass and short grasslands by the intermediate stature of the grassland layer. It is distinguished from the Central Forests/Grassland Transition Zone to the east by the relative scarcity of trees and shrubs. The major disturbance regimes are drought, the degree and frequency of grazing by domestic animals and wild ungulates, and fire.
The mixed grass prairie contains the floristic elements of the tall and short grass prairies and, combined with a rich forb flora, contains the highest floral complexity of any North American grassland ecoregion (Barbour et al. 1980). Typical grasses include little bluestem (Schyzachrium scoparium), western wheatgrass, (Agropyron smithii), and grama grasses (Bouteloua cartipendala). These species mix with taller grasses in the wetter areas and give way to shorter grasses in the drier areas (e.g., Bouteloua, Buchloe, Muhlenbergia, and Aristida) (Sims 1988). The effects of drought cycles and grazing intensity shift floristic composition to favor drought-tolerant species during dry periods and more shallow-rooted mesic loving plants during wetter periods. The Central and Southern Mixed Grasslands is among the top ten ecoregions in the number of reptile species and is an important breeding area for endemic Great Plains bird species. It also contains very important stopover sites for migratory birds, particularly on wetland sites scattered throughout this ecoregion. The Platte River Valley in Nebraska is a prominent area for sandhill cranes and the Cheyenne Bottoms in Kansas for populations of shorebirds during spring migration. Habitat Loss and Degradation Overall, only about 5 percent of the remaining habitat is considered to be intact. During the dustbowl of the 1930s, basal cover of grasses on even moderately grazed and heavily grazed grasslands declined from 80 percent or more to less than 10 percent in a period of 3-5 years (Sims 1988), but has since mostly regained its cover. Natural vegetation has been converted to cropland or pasture on about 90 percent of this ecoregion in Oklahoma and Texas. In Kansas and Nebraska, about 60 percent is in cropland and about 35 percent is grazed (USDA 1994). Remaining Blocks of Intact Habitat Most of the remaining blocks of intact habitat are quite small. Some of the most prominent include:
Degree of Fragmentation Much of the ecoregion that occurs in Kansas and Oklahoma still contains fragments of grassland associated with farms (i.e., unbroken sod). The remaining habitat in the rest of the ecoregion is fragmented. Degree of Protection With the exception of a high level of protection in the Wichita Mountains and Salt Plains, remaining habitat in the ecoregion is essentially unprotected. Types and Severity of Threats The major threat is conversion to agriculture. High wheat prices in the mid 1990s encouraged land conversion in western portions of the ecoregion. Center pivot irrigation has also caused conversion. Water flow into streams due to diversions is another problem. Fire apparently increases forage production in the eastern portion of this ecoregion, makes grasses more palatable, eliminates undesirable annuals, and suppresses the invasion of mesquite, juniper, and cacti (Wright and Bailey 1980). Thus, fire suppression constitutes another threat. Overgrazing by domestic stock, particularly in riparian areas, is a localized serious threat.
The Central and Southern Mixed Grasslands corresponds to Omernik (1995) ecoregion 27 (Central Plains Grasslands) and most of Küchler (1985) units 62 (Bluestem-grama prairie) and 76 (Mesquite-buffalograss). It also corresponds to Bailey (1994) sections 332E (South Central Great Plains), 311A (Redbed Plains), and 315C (Rolling Plains). Prepared by: Steve Chaplin, Terry Cook, Eric Dinerstein, Phillip Simms, and Karen Carney This text was originally published in the book Terrestrial ecoregions of North America: a conservation assessment from Island Press. This assessment offers an in-depth analysis of the biodiversity and conservation status of North America's ecoregions. All text by World Wildlife Fund © 2001 For more general information on this ecoregion, go to the WildWorld version of this description.
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